Abstract
High resolution Mars Orbiter Camera (MOC) images have revealed the existence of clusters of small cones in the Cerberus plains, Marte Valles, and Amazonis Planitia, Mars. These cones are similar in both morphology and planar dimensions to the larger of Icelandic rootless cones, which form due to explosive interactions between surficial lavas and near-surface groundwater. Impact crater size-frequency relationships indicate that surfaces upon which the cones sit are no older than 10 Ma. If martian cones form in the same manner as terrestrial rootless cones, then equatorial ground ice or ground water must have been present near the surface in geologically recent times.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 2365-2367 |
| Number of pages | 3 |
| Journal | Geophysical Research Letters |
| Volume | 28 |
| Issue number | 12 |
| DOIs | |
| State | Published - Jun 15 2001 |
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences
Fingerprint
Dive into the research topics of 'Rootless cones on Mars indicating the presence of shallow equatorial ground ice in recent times'. Together they form a unique fingerprint.Cite this
- APA
- Standard
- Harvard
- Vancouver
- Author
- BIBTEX
- RIS